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Convective heat and solute transfer in partially porous cavities

机译:部分多孔腔中的对流热和溶质传递

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This paper deals with natural convection driven by combined thermal and solutal buoyancy forces in a binary fluid. The configuration under study is a confined enclosure partially filled with a vertical porous layer. The mathematical description of the problem is based on a one-domain formulation of the conservation equations. The set of numerical results presented here quantitatively shows the influence of the porous layer on the flow structure and on heat and species transfer in the enclosure. The paper is focused on the analysis of the influence of the characteristic parameters governing double diffusive convection, namely the ratios of solutal and thermal parameters: the diffusivities and the buoyancy forces. Heat and mass transfer is analyzed as a function of the permeability of the porous layer. It is shown that the coupling of the flow penetration in the porous layer with the combined buoyancy forces induces a specific behavior of the flow structure and average heat transfer in the enclosure.
机译:本文涉及由二元流体中的热浮力和溶液浮力共同驱动的自然对流。研究中的配置是部分封闭有垂直多孔层的密闭外壳。问题的数学描述基于守恒方程的一域公式。此处呈现的一组数值结果定量地显示了多孔层对流动结构以及外壳中热量和物质传递的影响。本文着重分析支配双扩散对流的特征参数的影响,即溶质和热参数之比:扩散率和浮力。根据多孔层的渗透性分析传热和传质。结果表明,多孔层中的流动渗透与组合的浮力的耦合引起了流动结构的特定行为以及外壳中的平均热传递。

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